구상나무와 새로 발견(發見)된 품종(品種)

이창복,Lee, Tchang Bok 한국산림과학회 1970 한국산림과학회지 Vol.10 No.1

한라산에 자라는 구상나무는 4개의 품종으로 구성되었다. 이 중에서 푸른 구상나무와 붉은 구상나무는 학계에 새로 보고하는 것이기에 그의 원기재(原記載)와 더불어 발표한다. 검 구상나무는 지리산에서 발견된바 있으나 한라산에서는 이번이 처음이다. 목련나무의 대목(大木)도 여기에서 처음발견 되었다. Abies koreansa Wilson grows at the upper part of Mts. Halla, Chiri, Mudung, Kaji and Dokyu. It was at first collected by Father U. Faurie on the May of 1907 from the Mt. Halla, Quelpaert. Cone colour of this species varies from green to black purple and the typical colour of it is violet purple. A form of black purple was named by Hatushima in 1934. Green and reddish brown or reddish purple colours of this species were discovered recently at the Mt. Halla. All these forms can be identified as the following. for. koreana - Abies koreana Wilson in Journ. Arn. Arb. 1, 188(1920) ; Mori, En. 27(1922) ; Uyeki, Timb. Tr. 117(1926) et Woody Pl. 5(1940) ; Chung et al, Comm. Nam. 12(1937) ; Handb. Kor. Manch. For. 71(1939) ; Kawamoto, III. For. P1. 16(1940) ; T. Lee, Arb. Kor. 12(1947) et Billiogr. Woody P1. 233(1966) ; Nakai, Synopt. 23(1952)-A. nephrolepis sensu Nakai, Rep. Veg. Chirisan 23, no. 27(1915) et Rep. Veg. Quelpaert Isl. 13, no. 142 (1915), non Max. (1866) Strobili violaceo-purpurei, bracteis viridibus juvenilibus vel stramineis matureis. Mt. Halla ( Lee, no. 970527K. ) for. chlorocarpa, forma nova ; Strobili et bracteae viridi sed rubescent in apice juvenili inflerescentiae. Mt. Halla ( Lee, no. 970527C. ) for. rubrocarpa, forma nova ; Strobili et bracteae rubro-purpurei vel rubro-fusui Mt. Halla ( Lee, no. 970527R. ) for nigrocarpa Hatushima, Rep. Exp. For. Kyushu U. 40(1934) ; T. Lee, Arb. Kor. 12(1947) et Bibliogr. Woody P1,233(1966). Strobili et bracteae nigro-purpurei. Mt. Halla (Lee, no. 970527N. )

포항 로란-C (9930M) 신호를 이용한 ASF 해상측정

이창복,이종구,김영재,황상욱,이상정,양성훈,Lee, Chang-Bok,Lee, Jong-Koo,Kim, Young-Jae,Hwang, Sang-Wook,Lee, Sang-Jeong,Yang, Sung-Hoon 한국항해항만학회 2011 한국항해항만학회지 Vol. No.

Loran(LOang RAnge Navigation) 신호를 이용한 측위 시에 정확도에 가장 큰 영향을 미치는 오차요소는 TOA(Time of Arrival) 측정에서의 ASF(Additional Secondary Factor)이다. 따라서 공항접근이나 항만 접안 등의 측위 정확도를 만족시키려면 먼저 정확한 ASF측정이 선행되어야 하는데, 본 연구에서는 해상에서 ASF를 측정하는 기법을 연구하였다. 그 측정방법으로 포항 Loran-C 주국(9930M)에서 송신하는 로란 신호와 로란 수신기의 기준신호를 세슘원자시계를 기준으로 측정함으로써 해상에서의 ASF를 측정하였고 영일만 해상의 12 곳의 측정지점을 3 km 간격으로 설정하여 측정하였다. 해상측정에서 정확도를 높이기 위해서 전기장 안테나와 자기장 안테나를 동시에 사용하였으며 정확한 위치측정을 위해서 DGPS(Differential GPS)수신기를 이용하였다. 이런 방법을 이용하여 해상에서 ASF를 측정함으로써 ASF 예측값과 비교한 결과를 얻었다. A significant factor limiting the ranging accuracy of Loran (Long Range Navigation) signal is the additional secondary factor (ASF) in the time of arrival (TOA) measurements. Precise ASF values are essential if Loran deliver the high absolute accuracies demanded for aircraft approach, maritime harbour entrance. We measured the absolute propagation delay between Pohang Loran signal and Loran receiver output signal by comparing with Cesium atomic clock. In this study we measured ASFs between Pohang 9930M station and the 12 measurement points in the Yeongil Bay by using the measurement technique of absolute time delay. The measurement points were spaced at interval of 3 km by 3 km. An E-field antenna and an H-field antenna were used to improve the accuracy of ASF measurements and a DGPS (Differential GPS) receiver was used for accurate positions. We have gotten the result that the measured ASFs were compared with the predicted ASFs through this measurement technique.

미선나무 자생지(自生地) -특산자원(特産資源)으로서의 문화재(文化財)-

이창복,Lee, Chang-Bok 국립문화재연구원 1974 헤리티지:역사와 과학 Vol.8 No.-

농수산업 발전(農水産業 發展)의 세대적(世代的)인 길잡이

이창복,Lee, Chang-Bok 국립문화재연구원 1972 헤리티지:역사와 과학 Vol.6 No.-

한국 동남해역 대륙붕과 대륙사면 표면퇴적물의 분포와 특성

이창복,박용안,최진용,김기범,Lee, Chang-Bok,Park, Yong Ahn,Choi, Jin-Yong,Kim, Gi-Beom 한국해양학회 1989 韓國海洋學會誌 Vol.24 No.1

A total of 139 surface sediment samples, collected from the continental shelf and slope off the southeastern coast of Korea, were analyzed in order to understand their grain-size, mineral composition and organic carbon content. Based on the grain-size characteristics, five surface sedimentary facies were distinguished: sand, clay, mud, sand-mud mixed, and sand-clay mixed facies. The sand facies appears to be composed mostly of relict sand. For mud, most of which seem to be of recent origin, two different sources were suggested, based principally on their areal distribution pattern and the local hydrographic conditions. Heavy mineral composition of the fine-sand size fraction allowed us to distinguish different sand populations from the study area. On the whole, the Hupo Bank sediments showed a high content of garnet, while the sediments from the northern part of the continental shelf were characterized by a relatively high content of metamorphic minerals (kyanite, sillimanite, andalusite, staurolite). Among clay minerals, the most abundant was illite, with chlorite, kaolinite and smectite following in decreasing order. Organic carbon contents in the sediments of the study area were generally high and showed an average value of 1.94%. The sediment grain-size exerted a strong influence on the organic carbon content. The highest organic carbon content, on the other hand, was found in the continental slope sediments.

자원식물(資源植物)

이창복,Lee, Chang-Bok 한국산림과학회 1968 한국산림과학회지 Vol.8 No.1

GPS 위성을 이용한 시각비교 수신기의 개발

이창복,이동두,정낙삼,Lee, Chang-Bok,Lee, Dong-Doo,Chung, Nak-Sam 대한전자공학회 1990 전자공학회논문지 Vol. No.

정밀 시각비교를 위한 L1 대역(1575.42MHz), C/A 코드 GPS 수신기를 개발하여 성능평가를 하였다. 이 수신기를 이용하여 KSRI의 주 시계와 GPS 위성의 세슘 시계와의 GPS 측정을 100ns 이내의 정확도로 수행하였다. We have developed a L1 band (1575.42 MHz), C/A (Coarse/Acquisition) code GPS (Global Positioning System) receiver for precise time comparison and evaluated the performance of the receiver. The GPS measurements have been carried out between cesium clocks onboard the GPS satellites and the master clock of Korea Standards Research Institute (KSRI) using the GPS receiver. An accuracy of time transfer better than 100ns was obtained.

Sedimentology and Geochemical Properties of Intertidal Surface Sediments of the Banweol Area in the Southern Part of Kyeonggi Bay, Korea

이창복,박용안,고철환,Lee, Chang-Bok,Park, Yong-Ahn,Koh, Chul-Hwan The Korean Society of Oceanography 1985 韓國海洋學會誌 Vol.20 No.3

Sediment transport by tidal currents as well as the distribution and properties of intertial surface sediments are investigated using the data obtained from an anchor station on the main tidal channel and 56 tidal flat surface samples. Sedimentation in the intertidal zone appears to occur mainly during the spring tide period in this environment. The tidal flat can be classified into three depositional facies. The tidal flat deposits are ubiquitously bioturbated by various bottom dwelling organisms among which the crabs and polychaetes predominate. Average trace metal contents of the intertidal surface sediments are: 74.8 ppm co, 67.8 ppm Ni, 32.6 ppm Cu and 30.7 ppm Pb. Compared with the northen Kyeonggi Bay bottom sediments, these contents are significantly high, except for Pb.

광양만 표층퇴적물의 중금속 함량 및 분포

이창복,고철환,조영길,Lee, Chang-Bok,Koh, Chul-Hwan,Cho, Yeong-Gil 한국해양학회 2000 바다 Vol.5 No.2

광양만에서 채취된 91개 표층퇴적물에서 철, 망간, 크롬, 코발트, 구리, 니켈, 아연 및 납의 함량을 측정하였다. 분석된 금속 가운데 철, 크롬, 니켈 및 아연의 함량은 대부분의 시료에서 압도 의존적인 경향을 나타낸 반면 망간, 코발트, 구리 및 납은 입도와의 관련성이 뚜렷하지 않고 육지에 인접한 해역에서 국지적인 증가를 보였다. 평균입도, 유기탄소 및 각 금속을 변수로 한 R-mode 요인분석 결과도 철, 크롬, 니켈 및 아연이 입도, 유기탄소와함께 총 분산의 약 61%를 설명하는 factor 1에서 높은 적재값을 나타내 나머지 금속의 함량을 조절하는 요인과 구분되었다. 각 금속의 공간적 분포와 퇴적물의 입도, 유기탄소 및 금속간의 관련성 등을 종합적으로 검토한 결과 철, 크롬, 니켈 및 아연은 퇴적물의 입도에 의해서, 그리고 망간, 코발트, 구리 및 납은 해당 중금속의 배출과 관련된 해안 및 육지의 오염활동에 의해서 그 함량이 지배되는 것으로 파악되었다. 한편, 섬진강 부유물을 표준으로 삼아 계산된 농축비의 공간적 분포를 토대로 중금속의 축적이 활발한 지역이 구분되었는 바, 여수반도 북서쪽 연안에는 특히 아연 및 납이, 묘도 남수로를 포함한 여수반도 중북부 해안에는 망간, 코발트 및 구리가 농축된 것으로 드러났다. Heavy metals (Fe, Mn, Cr, Co, Cu, Ni, Zn, Pb) were determined in ninety-one surface sediments collected from Kwangyang Bay, south coast of Korea. The data show that the Fe, Cr, Ni, and Zn distribution in the bay can be described by metal vs. grain size relationship. However, the distribution pattern of Mn, Co, Cu and Pb were found to be changed because they are anthropogenically enriched to sediment. Correlation matrix and R-mode factor analyses revealed that two important factors controlling the distribution of metals in the bay are grain size and anthropogenic input.

조간대 퇴적물의 공극수 지구화학 : 1. 용존 영양염 (S, N, P)의 계절변화

이창복,김동선,Lee, Chang-Bok,Kim, Dong-Seon The Korean Society of Oceanography 1990 韓國海洋學會誌 Vol.25 No.1

A series of pore water data were obtained during the different time over one year period between October 1987 and October 1988, from a site on a muddy intertidal flat, located in the Kyeong-gi Bay, west coast of Korea, The results have revealed that the tidal flat is an environment of active nutrient the subface supplied by the overlying seawater is almost completely removed from the pore water at depth of about 10 cm below the sediment surface. The nutrients such as ammonium and phosphate are produced through this process and subsequently accumulated in the pore water forming steep gradients near the sediment surface. Below the main sulfate redirection zone, a secondary peak of dissolved sulfate was often observed. Greal seasonal variation of the pore water nutrient profiles was observed, which was particularly clear in their maximum concentration as well as in their concentration gradient. The rate constants of sulfate reduction and nutrient regeneration, estimated by using a diagenetic model (Berner, 1980), differ by an order of magnitude between the summer and winter seasons. The difference in sediment temperature may account for most of the calculated variation. The C:N:P ratio, calculated from the pore water nutrient gradients also exhibits a slight seasonal difference. The organic matter being decomposed by sulfate reduction appears to be depleted in depleted in nitrogen, compared to the average marine organic matter.